The north trend noted in forecast discussion:
Perhaps the most notable and significant feature affecting the
upcoming system is a compact shortwave diving southeast from the
Hudson Bay vicinity. This shortwave is rotating around a larger
cyclonic gyre centered over southeastern Canada near 60 W. This
upper pattern has acted to enhance confluence over northern New
England southward toward the Mid-Atlantic, which is resulting
in the more west to east low track out to sea to our south.
However, this shortwave feature to the north has appeared to
deepen a bit more than forecast over the last 12-24 hours,
resulting in subsequent subtle downstream height rises. It`s
not much, but it appears it may be just enough to weaken the
confluence near and to our north a touch, allowing a northward
shift in the tight northern edge of the snowfall from low
pressure passing to our south.
As such, 12z guidance has unanimously shifted northward. Mean
QPF from model output has risen to nearly an inch at the
southern most reaches of our CWA (southern Nelson County), and
just under a half inch near CHO. The northern edge of
accumulating snow remains a challenge, but there is a non-
zero/increasing chance for flurries or a light coating of snow
as far north as I-66/US-50, in line with the northern edge of a
baroclinic leaf developing upstream on satellite (marking the
northern edge of stronger synoptic upward motion).